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The Origin and Evolution of Mammals - Moodle

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50 THE ORIGIN AND EVOLUTION OF MAMMALS<br />

Figure 3.14 (continued).<br />

(d)<br />

(e) (f) (g)<br />

to 59, with a strong suspicion than several <strong>of</strong> these<br />

are still synonymous.<br />

Lystrosaurus (Fig. 3.14(c)) is the most remarkable<br />

pristerodontoid, indeed the most remarkable dicynodont<br />

in several ways. It is a tusked form clearly<br />

related to Dicynodon (Fig. 3.14(a)), but has exaggerated<br />

the shortening <strong>of</strong> both the palate <strong>and</strong> the<br />

temporal region <strong>of</strong> the skull, resulting in a strongly<br />

downturned snout. <strong>The</strong> Late Permian South African<br />

Kwazulusaurus (Fig. 3.14(b)) has a skull structure<br />

Kannemeyereria<br />

Tetragonius Stahleckeria Ischigualastia<br />

intermediate in form between Dicynodon <strong>and</strong><br />

Lystrosaurus <strong>and</strong> Maisch (2002) consequently interprets<br />

it as a basal lystrosaurid. Lystrosaurus itself is<br />

the only actual genus <strong>of</strong> dicynodont that is known<br />

to have survived the end-Permian, having been<br />

identified in the latest Permian as well as the earliest<br />

Triassic deposits (Smith 1995; King <strong>and</strong> Jenkins<br />

1997), when it became supremely abundant in terms<br />

<strong>of</strong> both numbers <strong>and</strong> geographical distribution.<br />

In South Africa, well over 90% <strong>of</strong> specimens

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